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    Flow over Heated Terrain. Part I: Linear Theory and Idealized Numerical Simulations

    Source: Monthly Weather Review:;2005:;volume( 133 ):;issue: 009::page 2552
    Author:
    Crook, N. Andrew
    ,
    Tucker, Donna F.
    DOI: 10.1175/MWR2964.1
    Publisher: American Meteorological Society
    Abstract: The flow past heated topography is examined with both linear and nonlinear models. It is first shown that the forcing of an obstacle with horizontally homogenous surface heating can be approximated by the forcing of an obstacle with surface heating isolated over the obstacle. The small-amplitude flow past an obstacle with isolated heating is then examined with a linear model. Under the linear approximation, the flow response to heated topography is simply the addition of the separate responses to thermal and orographic forcing. These separate responses are first considered individually and then the combined response is examined. Nondimensional parameters are developed that measure the relative importance of thermal and orographic forcing. Nonaxisymmetric forcing is then considered by examining the flow along and across a heated elliptically shaped obstacle. It is shown that the low-level lifting is maximized when the flow is along the major axis of the obstacle. The linear solutions are then tested in a nonlinear anelastic model. The response to a heat source and orography are first examined separately. Good agreement is found between nonlinear and linear models for the individual responses to thermal and orographic forcing. The case of uniformly heated flow past an obstacle is then examined. In these simulations, the thermal response is isolated by subtracting the orographic-only response from the full thermal?orographic response. The numerical simulations are able to capture the main features of the thermal response. Finally, numerical simulations of the flow along and across an elliptically shaped heated obstacle are examined, where it is verified that the lifting is maximized when the flow is along the major axis of the obstacle. These results are extended in Part II of this study to examine the moist convective response to flow over both idealized terrain and the complex terrain of the Rocky Mountains of the United States.
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      Flow over Heated Terrain. Part I: Linear Theory and Idealized Numerical Simulations

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4228966
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    contributor authorCrook, N. Andrew
    contributor authorTucker, Donna F.
    date accessioned2017-06-09T17:27:02Z
    date available2017-06-09T17:27:02Z
    date copyright2005/09/01
    date issued2005
    identifier issn0027-0644
    identifier otherams-85511.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228966
    description abstractThe flow past heated topography is examined with both linear and nonlinear models. It is first shown that the forcing of an obstacle with horizontally homogenous surface heating can be approximated by the forcing of an obstacle with surface heating isolated over the obstacle. The small-amplitude flow past an obstacle with isolated heating is then examined with a linear model. Under the linear approximation, the flow response to heated topography is simply the addition of the separate responses to thermal and orographic forcing. These separate responses are first considered individually and then the combined response is examined. Nondimensional parameters are developed that measure the relative importance of thermal and orographic forcing. Nonaxisymmetric forcing is then considered by examining the flow along and across a heated elliptically shaped obstacle. It is shown that the low-level lifting is maximized when the flow is along the major axis of the obstacle. The linear solutions are then tested in a nonlinear anelastic model. The response to a heat source and orography are first examined separately. Good agreement is found between nonlinear and linear models for the individual responses to thermal and orographic forcing. The case of uniformly heated flow past an obstacle is then examined. In these simulations, the thermal response is isolated by subtracting the orographic-only response from the full thermal?orographic response. The numerical simulations are able to capture the main features of the thermal response. Finally, numerical simulations of the flow along and across an elliptically shaped heated obstacle are examined, where it is verified that the lifting is maximized when the flow is along the major axis of the obstacle. These results are extended in Part II of this study to examine the moist convective response to flow over both idealized terrain and the complex terrain of the Rocky Mountains of the United States.
    publisherAmerican Meteorological Society
    titleFlow over Heated Terrain. Part I: Linear Theory and Idealized Numerical Simulations
    typeJournal Paper
    journal volume133
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR2964.1
    journal fristpage2552
    journal lastpage2564
    treeMonthly Weather Review:;2005:;volume( 133 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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